gsw_latentheat_evap_t

latent heat of evaporation

Contents

USAGE:

latentheat_evap_t = gsw_latentheat_evap_t(SA,t,p)

DESCRIPTION:

Calculates latent heat of evaporation of water from seawater 
(isobaric evaporation enthalpy) with in-situ temperature, t, as
input temperature at p = 0 (the surface).  It is defined as a 
function of Absolute Salinity, SA, and in-situ temperature, t, 
and is valid in the ranges 0 < SA < 40 g/kg and 0 < CT < 42 deg C.
The errors range between -0.4 and 0.6 J/kg.
TEOS-10 
Click for a more detailed description of calculating
latent heat of evaporation.

INPUT:

SA  =  Absolute Salinity                                        [ g/kg ]
t   =  in-situ temperature                                     [ deg C ]
SA & t need to have the same dimensions.

OUTPUT:

latentheat_evap_t  =  latent heat of evaporation                [ J/kg ]

EXAMPLE:

SA = [34.7118; 34.8915; 35.0256; 34.8472; 34.7366; 34.7324;]
t =  [28.7856; 28.4329; 22.8103; 10.2600;  6.8863;  4.4036;]
latentheat_evap_t = gsw_latentheat_evap_t(SA,t)
latentheat_evap_t =
  1.0e+006 *
   2.429882982734836
   2.430730236218543
   2.444217294049004
   2.474137411322517
   2.482156276375029
   2.488054617630297

AUTHOR:

Paul Barker, Trevor McDougall and Rainer Feistal    [ help@teos-10.org ]

VERSION NUMBER:

3.05 (16th February, 2015)

REFERENCES:

IOC, SCOR and IAPSO, 2010: The international thermodynamic equation of
 seawater - 2010: Calculation and use of thermodynamic properties.
 Intergovernmental Oceanographic Commission, Manuals and Guides No. 56,
 UNESCO (English), 196 pp.  Available from the TEOS-10 web site.
  See section 3.3 of this TEOS-10 Manual.
The software is available from http://www.TEOS-10.org